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Journal Article

How Sediment Supply, Sea-Level, and Glacial Isostatic Oscillations Drive Alluvial River Long-Profile Evolution and Terrace Formation

Authors
/persons/resource/aruby

Ruby,  Andreas       
Submitting Corresponding Author, Deutsches GeoForschungsZentrum;
4.6 Geomorphology, 4.0 Geosystems, Departments, GFZ Publication Database, GFZ Helmholtz Centre for Geosciences;

/persons/resource/mcnab

McNab,  Fergus       
4.6 Geomorphology, 4.0 Geosystems, Departments, GFZ Publication Database, GFZ Helmholtz Centre for Geosciences;

/persons/resource/tschild

Schildgen,  Taylor       
4.6 Geomorphology, 4.0 Geosystems, Departments, GFZ Publication Database, GFZ Helmholtz Centre for Geosciences;

/persons/resource/awickert

Wickert,  Andrew
4.6 Geomorphology, 4.0 Geosystems, Departments, GFZ Publication Database, GFZ Helmholtz Centre for Geosciences;

/persons/resource/milanez

Fernandes,  V. M.
4.6 Geomorphology, 4.0 Geosystems, Departments, GFZ Publication Database, GFZ Helmholtz Centre for Geosciences;

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5036499.pdf
(Publisher version), 28MB

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Citation

Ruby, A., McNab, F., Schildgen, T., Wickert, A., Fernandes, V. M. (2026): How Sediment Supply, Sea-Level, and Glacial Isostatic Oscillations Drive Alluvial River Long-Profile Evolution and Terrace Formation. - AGU Advances, 7, 1, e2025AV002035.
https://doi.org/10.1029/2025AV002035


Cite as: https://gfzpublic.gfz.de/pubman/item/item_5036499
Abstract
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